The Himalayan mountain: the Himalayan consist of three distinct parallel ranges. Longitudinally:
Great Himalayas/ himadri
Middle Himalayas/Himachal
Outer Himalayas/shiwalik
The Himalayan mountain: the Himalayas are geologically one of the youngest mountains in the world. The mountain range run in west-east direction from brahmaputra
great Himalayas or Himadri: this range is most continuous range consisting of the prominent peak with an average height of 6000m. important peaks are: mount everest (8848m), Kangchenjunga (8598m), nanda devi (7817m), and nanga parbat (8126m)
middle Himalaya or himachal: the south range of the great himalaya from the most rigged mountains. the latitude here is between 370-4500m. its width is 50km. important ranges are mahabharat, shimla, dalhousie, pir panjal, dharamshala
outer Himalayas or shiwalik: the outermost range of the Himalayas is called shiwalik. Their width ranges from 10-50km. they have altitudes between 900-1100m. the longitudinal trough/valley that is between the middle Himalayas as known as duns. it is a flat bottomed valleys covered with thick deposits of alluvium and gravel. eg. dehru dun, patli dun
the Himalaya are divided into four sections in the west-to-east direction:
the Kashmir/punjab Himalayas
the kumaun Himalaya
the nepal himalaya
the Assam Himalaya
Kashmir/Punjab Himalaya: between the Indus and Sutlej rivers.
kumaun Himalaya: between Sutlej and kali river
nepal himalaya: between kali and tista river
Assam Himalaya: between kali and Bharmaputra (dihong) rivers.
The Northern Plains: The interplay of three important river systems, the Indus, the Ganga and the Brahmaputra are plains called the Indo-Gangetic plains, along with the tributaries led to the formation of northern plains. this plain is a farm of alluvial fans.
alluvial fans are triangular-shaped deposits with their base facing the plain.
features formed by the river in the plain are:
bluff: a high, steep cliff used to donate a river-cut cliff or a steep slope
floodplain: a gentle slope formed by the layers of sediments deposited by the river over the floor of the valley
bar: a deposit of sand or mud in a river channel
channel: when a river gives a lot of mud and silt, it splits into a different direction.
levees: elevated banks, standing above the level of flood plains flanking a channel.
the vast northern plains can also be divided based on variation relief features into four regions:
khadar
bangar
terai
bhabar
khadar: the youngest alluvium deposits soil of flood plains
Bangar: the older alluvium deposits
terai: the wet marshy area having a thick forest and a variety of wildlife
bhabar: an 8-16km wide alluvium, that forms a pebble that is parallel to the slope of the river bed. lies among the feet of shiwaliks from indus to tista
the peninsular plateau: it is a tableland. it is composed of crystalline, igneous and metamorphic rock of old age. it was formed by the breaking up and drifting of the Godwanaland land. it is a part of the oldest landmass in India. this plateau has two broad division,
central highland
deccan plateau
Central highland
they lie to the north Narmada River
they are bounded by Vindhya mountain ranges
the chota nagpur plateau marks its eastern part
it slopes are west to east
elevation between 700-1000m
Deccan plateau
they lie in the south narmanda river
bounded by the eastern and western ghats
the mahadeo, kaimur hills and maikal range marks its eastern part
it slopes is from south to west to north east
elevation of 600m
in the western ghats, the highest peaks are anamudi (2695m) and doddabetta(2637m)
in the eastern ghats, the highest peaks are Mahendragiri (1,501 m)
The Malwa Plateau is located between Aravali and vindhya range
Escarpments are wall-like steep slopes of a ridge, forming a long barrier that rises higher than the surrounding land.
the Indian desert: the Indian desert lies towards the western Aravali hills. it is undulating with sand dunes. it receives very low rainfall below 150mm per year.
the Luni is the only large river in the region.
landforms of thar desert are divided into three major types:
sand covered thar
plains
hills
the coastal plains: a coastal plain is a low-lying and flat area of land that is near the coast and is adjacent to the sea coats. the coastal plains in India lay on either side of the Deccan plateau with the eastern and western coasts of India.
Western Coastal is divided into three sections:
Konkan coast: the highly rugged and dissected coastal plains in the north
Kannad Plain: the central sketch
Malabar coast: the third or southern sketch
estuaries: drowned valleys formed due to the rise in sea levels
lagoons: salt water lakes formed on the Kerala coast in the far south, eg, chilika lake
coromandel: the coast of southern Andhra Pradesh and Tamil Nadu
the island: Lakshadweep island group lying close to the Malabar coast of Kerala. it covers a small area of 32sq km. Kavaratti Island is the administrative headquarters of Lakshadweep
the andaman and Nicobar island is in the south. they are bigger in size and are more numerous and scattered
the Andaman and Nicobar Islands are a group of more than 3000 islands out of which 265 are uninhabitable.
the Lakshadweep Island were formed of coral deposits called atolls.
plate tectonic: the scientific concept that explains the movements of the crustal plates
folding: wrinkles and crumples of rock strata, caused by compression of the earths crust
split: a thin projection of land into the sea, lake or river; shell or reed extending from the shore